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GPI Anchoring of Proteins in the ER Membrane
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在矿物质含量中被困的Earchean生命元素
T Hassenkam1, M P Andersson1, K N Dalby1
1Nano-Science Center, Department of Chemistry, University of Copenhagen, Copenhagen 2100, Denmark.
Nature
|July 25, 2017
概括
格陵兰岩石中的古碳显示出早期生命的迹象. 石榴石晶体内的红外分析表明存在,氧和, 支持这些37亿年前的碳遗迹的生物起源.
科学领域:
- 地质化学
- 天体生物学
- 古生物学
背景情况:
- 西格陵兰岛伊沙岛的半沉积岩石年龄超过37亿年,含有13C贫的碳化合物.
- 这些古老的碳化合物有潜在的生物起源.
- 之前的研究缺乏其他与碳结合的基本生物元素的证据.
研究的目的:
- 来自伊沙的石榴 Porphyroblasts 内的碳含有物的元素组成.
- 确定其他生物元素 (N,O,P,H) 是否与古代碳结构相关.
- 提供可能是地球上最古老的生物碳遗迹的空间描述.
主要方法:
- 在现场使用红外吸收光谱.
- 分析的重点在于碳含中的大约10^-21 m^3区域.
- 这项研究检查了石榴石质细胞内装甲的内含物,以保持其完整性.
主要成果:
- 吸收光谱显示碳与和氧结合.
- 证据表明可能存在与碳结构结合的酸盐.
- 检测到低水平的C-H或O-H键,与热成熟的有机材料一致.
结论:
- 这些发现支持在37亿年前的伊沙土中发现的碳质物质的生物起源.
- 这项研究提供了证据,证明了地质构成中的Eoarchean有机残留物.
- 这些结果证实了地球最古老的地质记录中碳的生物起源.
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